the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Characterization and operation of a multi-channel Condensation Particle Counter (mc-CPC) for aircraft-based measurements
Abstract. Field measurements of aerosol number concentration and aerosol size distribution in the upper troposphere and lowermost stratosphere (UTLS) are crucial for understanding the influence of processes such as new particle formation (NPF) on aerosol budgets, cloud formation and climate. In this study, we present the multi-channel Condensation Particle Counter (mc-CPC) that was designed and constructed for airborne measurements and tested during the TPEx campaign onboard a Learjet in 2024. The instrument uses FC-43 (C12F27N) as the working fluid and consists of three individual CPCs (Grimm SKY-CPC), a pressure regulation system and a common inlet. By varying the temperature difference (ΔT) between each pair of saturator and condenser, the individual cutoff diameters (d50) of each CPC can be adjusted. For the cases presented here, we typically operated two of the CPCs at a ΔT of 36 °C for a direct comparison while the other CPC was set to a ΔT of 15 °C. Two independent calibration setups were used to determine the cutoff and size-dependent counting efficiency of the mc-CPC at various internal and external CPC pressure levels. The experiments in the laboratory showed that the cutoffs of the individual channels were rather independent of the external pressure pexternal and only slightly dependent on the internal CPC pressure pCPC, at least for a pCPC range between 200–350 hPa. A large fraction of flights during TPEx were conducted at an internal pressure of 250 hPa, and therefore the cutoff determined at 250 hPa was used as a fixed value for all internal pressures. For channel 1 and 2 that were operated at the same ΔT, this gave a d50 of 11.3 (±1.0) nm and 12.3 (±1.1) nm, respectively. Channel 3 was set to ΔT = 15°C and a cutoff diameter of 14.9 (±1.3) nm was determined. In an internal pressure range between 200 hPa and 400 hPa the cutoffs decreased slightly with increasing pCPC. Furthermore, our measurements also indicate that the cutoffs are not influenced by varying sample flows. The mc-CPC was operated for the first time on an aircraft during the TPEx campaign (TropoPause composition gradients and mixing Experiment) in June 2024. We present the first measurements of one research flight and discuss the uncertainties of the collected aerosol data.
Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Measurement Techniques.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.- Preprint
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- RC1: 'Comment on egusphere-2025-4349', Anonymous Referee #1, 09 Oct 2025
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RC2: 'Comment on egusphere-2025-4349', Anonymous Referee #2, 16 Oct 2025
Excellent work in characterizing and correcting the performance of the CPC during non-ideal cases, such as unknown/uncontrolled sample flow and varying external and instrument pressures. There’s a lot of normalization that is happening that probably warrants a summation of error bars to understand the compounding corrections applied to the field dataset. The equation determining NPF is maybe overly strict, but also seems arbitrary as it's currently written. Considering this is the major focus of the instrument, I think this needs better justification or characterization. I think the combination of the aforementioned error analyses and Poisson variance would provide a stronger basis for quantifying NPF. Without the inlet pressure control being appropriately designed and characterized, the instrument may not accurately indicate the total particle number concentration, but is sufficient for NPF quantification since common-mode errors of larger particle loss is subtracted. This can be easily remedied in the next instrument update, to improve the amount of information received. Similarly, the second channel can be put to better use gathering additional information instead of redundant with the first channel.
L020: Why was flight 4 selected when it was operated at a different pressure from typical?
L089: Suggest changing “gets mixed” to “mixes” for succinctness.
L090: Suggest changing “enable” to “causing” or “activating”, showing causality.
L101: Critical orifice is not shown in Figure 1 flow diagram. Is it within the Channel block? What is the role of the pump valve if not for flow control?
L221: Correcting for inlet orifice particle loss isn’t necessary if only subtracting channels for an NPF measurement, but it is critical if trying to observe total particle concentration, especially in the lower Stratosphere, where mode size is typically accumulation mode. During ACCLIP, the integrated UHSAS concentration often exceeded the NMASS concentration in the Stratosphere due to losses in the pressure control orifice. Losses can be reduced with an appropriately designed expansion section after the orifice.
L241: Eqn. 2 values seem arbitrary. Some of the cited papers use different values for uncertainty. Recommend testing analysis from Williamson et al., 2019 with your dataset based on Poisson counting statistics.
L328: What was the DMA sample flow? Relevant to understanding transfer function width (and thus horizontal error bars in the sizing).
Fig 4: Can you clarify how the error bars are calculated? Is it the standard deviation from the varying particle number concentration measured during the time period of each test point? Is the standard deviation of the TSI reference CPC considered, since it will fluctuate as well. In Poisson statistics, need to sum variances together.
L472: This would not be a factor for sub-100 nm particles if an expansion section was included.
Fig 7: I think it would be nice to see the effect that pressure has on the plateau efficiency, rather than the normalized plots.
Table 4: Is Ch3 operating temperature a typo, or did you operate Ch3 at dT=36C? If so, why did you calibrate the counting efficiency outside of its operating spec? And why is D50 of CPC3 relatively high for the same dT?
Fig 9: How can you have N11-N15 ~= 1000 /scm3 and consider it “no NPF”? This circles back to my comments on Eqn. 2. The whole section from 12:30-13:45 looks strongly related to NPF.
L627: Is the inlet pressure reduction orifice properly sized for 200 hPa operation? Maybe you can go smaller and switch at a higher altitude to reduce amount of bypass flow the pump has to accommodate.
L641: The diffusion losses of 10-13 nm can be corrected since you have that information from subtracting the two channels and their relative contribution to the total concentration.
Instrument suggestions for future development: Designing and characterizing an appropriate expansion chamber at the inlet pressure control orifice will allow the first channel to (closer) measure a total number concentration. Now that the first and second channel have been tested together, I think the first channel alone can be trusted, so the second channel can be used for additional information such as a third cut size or a non-volatile measurement (if inlet orifice is characterized through Accumulation mode).
Citation: https://doi.org/10.5194/egusphere-2025-4349-RC2
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This paper presents a description of an aircraft-based, multi-channel condensation particle counter (mc-CPC) used for investigating the new particle formation (NPF) in the UTLS. They provide a detailed description of the system design and the careful, comprehensive calibrations, with an example of in-flight data from the TPEx campaign on tropopause composition in 2024. This mc-CPC system was developed by integrating three commercial GRIMM SKY-CPCs with a custom-built pressure regulation and flow manifold for aircraft-based measurements. FC-43 was used as the working fluid, which, according to the authors, was tested for the first time on Grimm SKY-CPC. The mc-CPC system consists of three channels to provide two size cuts, ~11-12 nm (chan1 and chan2) and ~15 nm (chan3). The counting efficiency of the CPC was corrected for flow and pressure, but not for the particle loss through the inlet and sampling line. The comparative use of the two size cuts from the mc-CPC (i.e., the difference between the particle number concentrations of the low and high size cuts) provides identification of NPF events.
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